
mineral
Tumbled chalcedony or jasper
Microcrystalline quartz (SiO₂), likely iron-bearing chalcedony/jasper
AI-generated identification · may be incorrectSmooth, rounded, translucent-to-opaque brown-gray stone with tiny reddish inclusions and a vitreous-to-waxy luster. Hardness is about 6.5–7 Mohs; quartz has no cleavage and a cryptocrystalline structure.
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Physical properties
Smooth, rounded, translucent-to-opaque brown-gray stone with tiny reddish inclusions and a vitreous-to-waxy luster. Hardness is about 6.5–7 Mohs; quartz has no cleavage and a cryptocrystalline structure.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures, later incorporating iron oxides and other impurities; specimens may range from volcanic-host-rock ages to younger alluvial deposits. Tumbling has produced the polished surface.
Uses & applications
Used for cabochons, beads, carvings, lapidary pieces, and inexpensive collectibles; quality depends on color, pattern, translucency, and finish.
Geological facts
The exact variety cannot be confirmed from one photograph; it could also be a brown agate, jasper, or iron-stained quartz pebble.
Field identification & locations
Field clues include quartz-like hardness, resistance to scratching by steel, and a smooth waxy fracture; it commonly occurs in volcanic regions, gravel beds, and stream deposits. A streak, specific-gravity, or microscopic examination would improve identification.
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